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The vertical structure of temperature and humidity fields in the atmospheric boundary layer over Western Siberia in clear air and in the presence of continuous cloudiness

  • Atmospheric Radiation, Optical Weather, and Climate
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Abstract

The peculiarities of the vertical structures of temperature and water vapor mass fraction fields in the atmospheric boundary layer of Western Siberia typical for clear air and continuous cloudiness of the lower layer are discussed.

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References

  1. K. Ya. Kondrat’ev and Yu. M. Timofeev, Meteorological Sensing of the Atmosphere from Space (Gidrometeoizdat, Leningrad, 1978) [in Russian].

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  2. V. E. Zuev and V. V. Zuev, Remote Optical Sensing of the Atmosphere (Gidrometeoizdat, St. Petersburg, 1992) [in Russian].

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  3. V. S. Komarov and N. Ya. Lomakina, Statistical Models of Atmosphere Boundary Layer of Western Siberia (IOA SO RAN, Tomsk, 2008) [in Russian].

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Authors and Affiliations

  1. Zuev Institute of Atmospheric Optics, Siberian Branch, Russian Academy of Sciences, pl. Akademika Zueva 1, Tomsk, 634021, Russia

    V. S. Komarov, N. Ya. Lomakina & S. N. Il’in

Authors
  1. V. S. Komarov
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  2. N. Ya. Lomakina
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  3. S. N. Il’in
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Corresponding author

Correspondence to V. S. Komarov.

Additional information

Original Russian Text © V.S. Komarov, N.Ya. Lomakina, S.N. Il’in, 2010, published in Optica Atmosfery i Okeana.

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Komarov, V.S., Lomakina, N.Y. & Il’in, S.N. The vertical structure of temperature and humidity fields in the atmospheric boundary layer over Western Siberia in clear air and in the presence of continuous cloudiness. Atmos Ocean Opt 23, 28–31 (2010). https://doi.org/10.1134/S1024856010010069

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  • DOI: https://doi.org/10.1134/S1024856010010069

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